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Olsen, L.M., G. Major, K. Shein, J. Scialdone, S. Ritz, T. Stevens, M. Morahan, A. Aleman, R. Vogel, S. Leicester, H. Weir, M. Meaux, S. Grebas, C.Solomon, M. Holland, T. Northcutt, R. A. Restrepo, R. Bilodeau, 2013. NASA/Global Change Master Directory (GCMD) Earth Science Keywords. Version 8.0.0.0.0 ← back Released Dataset MED-SUV CUBE arrays 2014 – Datasets Cite as: Copy citation to clipboard Pilz, Marko; Woith, Heiko; Festa, Gaetano (2018): MED-SUV CUBE arrays 2014 – Datasets. GFZ Data Services. https://doi.org/10.5880/GIPP.201403.1 Status I N R E V I E W : Pilz, Marko; Woith, Heiko; Festa, Gaetano (2018): MED-SUV CUBE arrays 2014 – Datasets. GFZ Data Services. https://doi.org/10.5880/GIPP.201403.1
Abstract This data set contains continuous recordings of seismic noise, which have been made on the surface of a shallow volcanic crater in the Phlegrean Fields volcanic complex near Naples, Italy, where a significant level of volcanic-hydrothermal activity is presently concentrated (MED-SUV = Mediterranean Supersite Volcanoes). As part of the Phlegrean Fields, the Solfatara crater is a 0.4 × 0.5 km sub-rectangular structure whose geometry is mainly due to the control exerted by N40–50W and N50E trending normal fault systems, along which geothermal fluids can ascend. These systems crosscut the study area and have been active several times in the past
Authors Pilz, Marko;GFZ German Research Centre for Geosciences, Potsdam, Germany Woith, Heiko ;GFZ German Research Centre for Geosciences, Potsdam, GermanyFesta, Gaetano;Università di Napoli Federico II, Naples, Italy Contact Contributors GIPP Support Team
Keywords earth science, tectonics, volcanic activity, seismic noise, arrays, PASSIVE_SEISMIC > NETWORK, SENSOR > GEOPHONE, SENSOR > 3-C, LAND, MINISEED_DATA_FORMAT, SEISMIC_WAVEFORM_DATA More Metadata datacite:
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As part of the Phlegrean Fields, the Solfatara crater is a 0.4 × 0.5 km sub-rectangular structure whose geometry is mainly due to the control exerted by N40–50W and N50E trending normal fault systems, along which geothermal fluids can ascend. 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